Premium
The Landslide Hazard Chain in the Tapovan of the Himalayas on 7 February 2021
Author(s) -
Jiang Ruochen,
Zhang Limin,
Peng Dalei,
He Xin,
He Jian
Publication year - 2021
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2021gl093723
Subject(s) - debris flow , landslide , erosion , hydropower , geology , flood myth , debris , deposition (geology) , hydrology (agriculture) , hazard analysis , geomorphology , physical geography , geotechnical engineering , geography , oceanography , sediment , archaeology , engineering , aerospace engineering , electrical engineering
On February 7, 2021, a catastrophic landslide occurred in Chamoli, India on the southern hills of the Himalayas ( 30.37 ° N, 79.73 ° E). About 28 × 10 6 m 3 of landslide mass detached from the mountain face, entrained deposits in the valley and riverbed, and generated a huge debris flood along the Dhauliganga River. In this study, the geomorphological and volumetric characteristics of the disaster chain were interpreted from satellite images. The full process of the disaster chain and the erosion, deposition and flow discharge processes were reproduced using a cell‐based analysis program, Erosion–Deposition Debris Flow Analysis (EDDA). The results indicate a peak flow discharge of the debris flood at Tapovan Hydropower Station of about 25,000–28,000 m 3 /s. The main erosion and deposition zones are distributed along the valley floor and the Dhauliganga River, respectively. This study serves as basis for understanding the disaster chain dynamics in high mountain areas.